The diagram shows a cross section of Earth and the layers of Earth's Interior. The diagram also shows the paths of earthquake waves moving through Earth. These paths were determined by selsmographs detecting the various types of waves reaching points all around the surface of Earth
at different times.
SS
SKS
SKE
Source of
Earthquake
Surface waves
Inner Core
Outer Core
Lower Mantle
Upper Mantle
Crust
PKS
How were earthquake waves able to help geologists determine the different layers of Earth's interior?
O A. Waves traveled at different speeds through different substances Inside Earth.
O B. Geologists determined the depths of layers when the waves were reflected back to the source.
O c. Layers of Earth increased the amplitude of the earthquake waves making them easier to detect.
OD. Earthquake waves made the layers softer allowing geologists to drill shafts down to the inner layers.

B. Geologists determined the depths of layers when the waves were reflected back to the source.

answer:

the water molecules are transferred from the roots to the stem or top parts of the tall tree because of important properties of water which are adhesion, cohesion and capillary action. cohesion is the property of water molecules keeps water molecules in a combined state by sharing of bonds between them at the atomic level. adhesion allows the interaction of water molecules with other substances or substrate. adhesion will cause the attachment of water molecules to the wall of the vessel (xylem) of the plant. capillary action occurs when the adhesive force to the vessel wall is stronger than the cohesive force between water molecules. capillary action mimics the transfer of water from a tube or pipe. in this way water utilizes its property to transfer water from down to top level of the plant.